FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2006488049> ?p ?o ?g. }

• W2006488049 endingPage "393" @default.
• W2006488049 startingPage "383" @default.
• W2006488049 abstract "The parallel physically-based surface–subsurface model PARFLOW was used to investigate the spatial patterns and temporal dynamics of river–aquifer exchange in a heterogeneous alluvial river–aquifer system with deep water table. Aquifer heterogeneity at two scales was incorporated into the model. The architecture of the alluvial hydrofacies was represented based on conditioned geostatistical indicator simulations. Subscale variability of hydraulic conductivities (K) within hydrofacies bodies was created with a parallel Gaussian simulation. The effects of subscale heterogeneity were investigated in a Monte Carlo framework. Dynamics and patterns of river–aquifer exchange were simulated for a 30-day flow event. Simulation results show the rapid formation of saturated connections between the river channel and the deep water table at preferential flow zones that are characterized by high conductivity hydrofacies. Where the river intersects low conductivity hydrofacies shallow perched saturated zones immediately below the river form, but seepage to the deep water table remains unsaturated and seepage rates are low. Preferential flow zones, although only taking up around 50% of the river channel, account for more than 98% of total seepage. Groundwater recharge is most efficiently realized through these zones. Subscale variability of Ksat slightly increased seepage volumes, but did not change the general seepage patterns (preferential flow zones versus perched zones). Overall it is concluded that typical alluvial heterogeneity (hydrofacies architecture) is an important control of river–aquifer exchange in rivers overlying deep water tables. Simulated patterns and dynamics are in line with field observations and results from previous modeling studies using simpler models. Alluvial heterogeneity results in distinct patterns and dynamics of river–aquifer exchange with implications for groundwater recharge and the management of riparian zones (e.g. river channel-floodplain connectivity via saturated zones)." @default.
• W2006488049 created "2016-06-24" @default.
• W2006488049 creator A5008417002 @default.
• W2006488049 creator A5010959379 @default.
• W2006488049 creator A5015563464 @default.
• W2006488049 creator A5042614830 @default.
• W2006488049 date "2009-09-01" @default.
• W2006488049 modified "2023-10-10" @default.
• W2006488049 title "Patterns and dynamics of river–aquifer exchange with variably-saturated flow using a fully-coupled model" @default.
• W2006488049 cites W1494527298 @default.
• W2006488049 cites W1508635819 @default.
• W2006488049 cites W1542622005 @default.
• W2006488049 cites W1637881687 @default.
• W2006488049 cites W1643292166 @default.
• W2006488049 cites W1643537079 @default.
• W2006488049 cites W1657608520 @default.
• W2006488049 cites W1915946256 @default.
• W2006488049 cites W1967008259 @default.
• W2006488049 cites W1976159327 @default.
• W2006488049 cites W1982144177 @default.
• W2006488049 cites W1989925771 @default.
• W2006488049 cites W1996595352 @default.
• W2006488049 cites W1999973399 @default.
• W2006488049 cites W2004502141 @default.
• W2006488049 cites W2006631142 @default.
• W2006488049 cites W2007105038 @default.
• W2006488049 cites W2014357777 @default.
• W2006488049 cites W2029144448 @default.
• W2006488049 cites W2033116373 @default.
• W2006488049 cites W2035444434 @default.
• W2006488049 cites W2043140308 @default.
• W2006488049 cites W2053133753 @default.
• W2006488049 cites W2062478360 @default.
• W2006488049 cites W2070685888 @default.
• W2006488049 cites W2073867489 @default.
• W2006488049 cites W2076001950 @default.
• W2006488049 cites W2084341227 @default.
• W2006488049 cites W2085396229 @default.
• W2006488049 cites W2086651486 @default.
• W2006488049 cites W2087520869 @default.
• W2006488049 cites W2094092185 @default.
• W2006488049 cites W2095967021 @default.
• W2006488049 cites W2096821779 @default.
• W2006488049 cites W2112981866 @default.
• W2006488049 cites W2115611895 @default.
• W2006488049 cites W2131534978 @default.
• W2006488049 cites W2133983843 @default.
• W2006488049 cites W2134424445 @default.
• W2006488049 cites W2165202893 @default.
• W2006488049 cites W2326531020 @default.
• W2006488049 doi "https://doi.org/10.1016/j.jhydrol.2009.06.038" @default.
• W2006488049 hasPublicationYear "2009" @default.
• W2006488049 type Work @default.
• W2006488049 sameAs 2006488049 @default.
• W2006488049 citedByCount "96" @default.
• W2006488049 countsByYear W20064880492012 @default.
• W2006488049 countsByYear W20064880492013 @default.
• W2006488049 countsByYear W20064880492014 @default.
• W2006488049 countsByYear W20064880492015 @default.
• W2006488049 countsByYear W20064880492016 @default.
• W2006488049 countsByYear W20064880492017 @default.
• W2006488049 countsByYear W20064880492018 @default.
• W2006488049 countsByYear W20064880492019 @default.
• W2006488049 countsByYear W20064880492020 @default.
• W2006488049 countsByYear W20064880492021 @default.
• W2006488049 countsByYear W20064880492022 @default.
• W2006488049 countsByYear W20064880492023 @default.
• W2006488049 crossrefType "journal-article" @default.
• W2006488049 hasAuthorship W2006488049A5008417002 @default.
• W2006488049 hasAuthorship W2006488049A5010959379 @default.
• W2006488049 hasAuthorship W2006488049A5015563464 @default.
• W2006488049 hasAuthorship W2006488049A5042614830 @default.
• W2006488049 hasConcept C114793014 @default.
• W2006488049 hasConcept C127313418 @default.
• W2006488049 hasConcept C131227075 @default.
• W2006488049 hasConcept C159390177 @default.
• W2006488049 hasConcept C159750122 @default.
• W2006488049 hasConcept C174091901 @default.
• W2006488049 hasConcept C187320778 @default.
• W2006488049 hasConcept C39769621 @default.
• W2006488049 hasConcept C63184880 @default.
• W2006488049 hasConcept C69823785 @default.
• W2006488049 hasConcept C75622301 @default.
• W2006488049 hasConcept C76177295 @default.
• W2006488049 hasConcept C76886044 @default.
• W2006488049 hasConceptScore W2006488049C114793014 @default.
• W2006488049 hasConceptScore W2006488049C127313418 @default.
• W2006488049 hasConceptScore W2006488049C131227075 @default.
• W2006488049 hasConceptScore W2006488049C159390177 @default.
• W2006488049 hasConceptScore W2006488049C159750122 @default.
• W2006488049 hasConceptScore W2006488049C174091901 @default.
• W2006488049 hasConceptScore W2006488049C187320778 @default.
• W2006488049 hasConceptScore W2006488049C39769621 @default.
• W2006488049 hasConceptScore W2006488049C63184880 @default.
• W2006488049 hasConceptScore W2006488049C69823785 @default.
• W2006488049 hasConceptScore W2006488049C75622301 @default.
• W2006488049 hasConceptScore W2006488049C76177295 @default.
• W2006488049 hasConceptScore W2006488049C76886044 @default.

• next